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Geological Survey
DEPABTMENT OF THE INTEKIOR BULLETIN OF THE UNITED STATES GEOLOGICAL SURVEY N~o. 151 WASHINGTON GOVERNMENT PRINTING OFFICE 1898 UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIEECTOR THE LOWER CRETACEOUS GRYPMAS OF THK TEX.AS REGION ROBERT THOMAS HILL THOMAS WAYLA'ND VAUGHAN WASHINGTON GOVERNMENT FEINTING OFFICE 18.98 THE LOWER CRETACEOUS GRYPHJ1AS OF THE TEXAS REGION. BY I EOBEET THOMAS HILL and THOMAS WAYLAND VAUGHAN. CONTENTS. Page. Letter of transmittal....._..........._....._ ............................ 11 Introduction ...---._._....__................._....._.__............._...._ 13 The fossil oysters of the Texas region.._._.._.___._-..-._._......-..--.... 23 Classification of the Ostreidae. .. ...-...---..-.......-.....-.-............ 24 Historical statement of the discovery in the Texas region of the forms referred to Gryphsea pitcher! Morton ................................ 33 Gryphaea corrugata Say._______._._..__..__...__.,_._.________...____.._ 33 Gryphsea pitcheri Morton............................................... 34 Roemer's Gryphsea pitcheri............................................ 35 Marcou's Gryphsea pitcheri............................................ 35 Blake's Gryphaea pitcheri............................................. 36 Schiel's Gryphsea pitcheri...........................,.:................ 36 Hall's Gryphsea pitcheri (= G. dilatata var. tucumcarii Marcou) ...... 36 Heilprin's Gryphaea pitcheri.....'..................................... 37 Gryphaea pitcheri var. hilli Cragin................................... -
Comprehensive Review of Cambrian Himalayan
http://www.diva-portal.org Postprint This is the accepted version of a paper published in Papers in Palaeontology. This paper has been peer- reviewed but does not include the final publisher proof-corrections or journal pagination. Citation for the original published paper (version of record): Popov, L E., Holmer, L E., Hughes, N C., Ghobadi Pour, M., Myrow, P M. (2015) Himalayan Cambrian brachiopods. Papers in Palaeontology, 1(4): 345-399 http://dx.doi.org/10.1002/spp2.1017 Access to the published version may require subscription. N.B. When citing this work, cite the original published paper. Permanent link to this version: http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-255813 HIMALAYAN CAMBRIAN BRACHIOPODS BY LEONID E. POPOV1, LARS E. HOLMER2, NIGEL C. HUGHES3 MANSOUREH GHOBADI POUR4 AND PAUL M. MYROW5 1Department of Geology, National Museum of Wales, Cathays Park, Cardiff CF10 3NP, United Kingdom, <[email protected]>; 2Institute of Earth Sciences, Palaeobiology, Uppsala University, SE-752 36 Uppsala, Sweden, <[email protected]>; 3Department of Earth Sciences, University of California, Riverside, CA 92521, USA <[email protected]>; 4Department of Geology, Faculty of Sciences, Golestan University, Gorgan, Iran and Department of Geology, National Museum of Wales, Cathays Park, Cardiff CF10 3NP, United Kingdom <[email protected]>; 5 Department of Geology, Colorado College, Colorado Springs, CO 80903, USA <[email protected]> Abstract: A synoptic analysis of previously published material and new finds reveals that Himalayan Cambrian brachiopods can be referred to 18 genera, of which 17 are considered herein. These contain 20 taxa assigned to species, of which five are new: Eohadrotreta haydeni, Aphalotreta khemangarensis, Hadrotreta timchristiorum, Prototreta? sumnaensis and Amictocracens? brocki. -
United States
DEPARTMENT OF THE INTERIOR BULLETIN OF THE UNITED STATES ISTo. 146 WASHINGTON GOVERNMENT Pit IN TING OFFICE 189C UNITED STATES GEOLOGICAL SURVEY CHAKLES D. WALCOTT, DI11ECTOK BIBLIOGRAPHY AND INDEX NORTH AMEEICAN GEOLOGY, PALEONTOLOGY, PETEOLOGT, AND MINERALOGY THE YEA.R 1895 FEED BOUGHTON WEEKS WASHINGTON Cr O V E U N M K N T P K 1 N T I N G OFFICE 1890 CONTENTS. Page. Letter of trail smittal...... ....................... .......................... 7 Introduction.............'................................................... 9 List of publications examined............................................... 11 Classified key to tlio index .......................................... ........ 15 Bibliography ............................................................... 21 Index....................................................................... 89 LETTER OF TRANSMITTAL DEPARTMENT OF THE INTEEIOE, UNITED STATES GEOLOGICAL SURVEY, DIVISION OF GEOLOGY, Washington, D. 0., June 23, 1896. SIR: I have the honor to transmit herewith the manuscript of a Bibliography and Index of North American Geology, Paleontology, Petrology, and Mineralogy for the year 1895, and to request that it be published as a bulletin of the Survey. Very respectfully, F. B. WEEKS. Hon. CHARLES D. WALCOTT, Director United States Geological Survey. 1 BIBLIOGRAPHY AND INDEX OF NORTH AMERICAN GEOLOGY, PALEONTOLOGY, PETROLOGY, AND MINER ALOGY FOR THE YEAR 1895. By FRED BOUGHTON WEEKS. INTRODUCTION. The present work comprises a record of publications on North Ameri can geology, paleontology, petrology, and mineralogy for the year 1895. It is planned on the same lines as the previous bulletins (Nos. 130 and 135), excepting that abstracts appearing in regular periodicals have been omitted in this volume. Bibliography. The bibliography consists of full titles of separate papers, classified by authors, an abbreviated reference to the publica tion in which the paper is printed, and a brief summary of the con tents, each paper being numbered for index reference. -
OREGON ESTUARINE INVERTEBRATES an Illustrated Guide to the Common and Important Invertebrate Animals
OREGON ESTUARINE INVERTEBRATES An Illustrated Guide to the Common and Important Invertebrate Animals By Paul Rudy, Jr. Lynn Hay Rudy Oregon Institute of Marine Biology University of Oregon Charleston, Oregon 97420 Contract No. 79-111 Project Officer Jay F. Watson U.S. Fish and Wildlife Service 500 N.E. Multnomah Street Portland, Oregon 97232 Performed for National Coastal Ecosystems Team Office of Biological Services Fish and Wildlife Service U.S. Department of Interior Washington, D.C. 20240 Table of Contents Introduction CNIDARIA Hydrozoa Aequorea aequorea ................................................................ 6 Obelia longissima .................................................................. 8 Polyorchis penicillatus 10 Tubularia crocea ................................................................. 12 Anthozoa Anthopleura artemisia ................................. 14 Anthopleura elegantissima .................................................. 16 Haliplanella luciae .................................................................. 18 Nematostella vectensis ......................................................... 20 Metridium senile .................................................................... 22 NEMERTEA Amphiporus imparispinosus ................................................ 24 Carinoma mutabilis ................................................................ 26 Cerebratulus californiensis .................................................. 28 Lineus ruber ......................................................................... -
Sucesión De Amonitas Del Cretácico Superior (Cenomaniano – Coniaciano) De La Parte Más Alta De La Formación Hondita Y De L
Boletín de Geología Vol. 33, N° 1, enero-junio de 2011 SUCESIÓN DE AMONITAS DEL CRETÁCICO SUPERIOR (CENOMANIANO – CONIACIANO) DE LA PARTE MÁS ALTA DE LA FORMACIÓN HONDITA Y DE LA FORMACIÓN LOMA GORDA EN LA QUEBRADA BAMBUCÁ, AIPE - HUILA (COLOMBIA, S. A.) Pedro Patarroyo1 RESUMEN La sección de la quebrada Bambucá (Aipe - Huila) posee una buena exposición de los depósitos del Cretácico del Valle Superior del Magdalena. De la parte alta de la Formación Hondita se recolectaron Acanthoceras sp. y Rhynchostreon sp. del Cenomaniano superior. Dentro del segmento inferior de la Formación Loma Gorda se hallaron Choffaticeras (C.) cf. segne, Fagesia cf. catinus, Neoptychites cf. andinus, Mitonia gracilis, Morrowites sp., Nannovascoceras ? sp., Quitmaniceras ? sp., Benueites ? sp. junto con Mytiloides kossmati, M. goppelnensis y Anomia sp. del Turoniano inferior. Estratigráficamente arriba aparecen Paramammites ? sp., Hoplitoides sp. H. ingens, H. cf. lagiraldae, Codazziceras ospinae, Allocrioceras sp., que pueden estar representando entre el Turoniano inferior y medio. Para la parte alta de este segmento se encontraron Prionocycloceras sp. P. guayabanum, Reesidites subtuberculatum, Subprionotropis colombianus, Mytiloides scupini, Dydimotis sp., Gauthiericeras sp., Anagaudryceras ? sp., Eulophoceras jacobi, Paralenticeras sieversi, Hauericeras cf. madagascarensis, Peroniceras (P.) subtricarinatum, Forresteria (F.) sp., Barroisiceras cf. onilahyense, Ankinatsytes venezolanus que abarcan entre el Turoniano superior y el Coniaciano. Con base en la fauna colectada no es posible establecer los límites Cenomaniano/Turoniano y Turoniano/Coniaciano. Palabras clave: Amonitas, Cretácico superior, Valle Superior del Magdalena, Aipe-Huila-Colombia. UPPER CRETACEOUS AMMONITE SUCCESSION (CENOMANIAN – CONIACIAN) RELATED TO THE UPPER HONDITA AND LOMA GORDA FORMATIONS ALONG THE BAMBUCÁ CREEK, AIPE - HUILA (COLOMBIA, S.A.) ABSTRACT The Bambucá creek section (Aipe - Huila) shows a very good exposition of the Upper Magdalena Valley Cretaceous deposits. -
Pectínidos Pliocenos De La Cuenca De Vejer (Cádiz, So De España)
ISSN: 0211-8327 Studia Geologica Salmanticensia, 44 (1): pp. 91-140 PECTÍNIDOS PLIOCENOS DE LA CUENCA DE VEJER (CÁDIZ, SO DE ESPAÑA) [Pliocene pectinids from the Vejer Basin (Cadiz, SW Spain)] Alberto RICO-GARCÍA (*) (*): Departamento de Geología. Universidad de Salamanca. Facultad de Ciencias. Plaza de la Merced, s/n. 37008 Salamanca. Correo-e: [email protected] (FECHA DE RECEPCIÓN: 2008-04-01) (FECHA DE ADMISIÓN: 2008-04-15) BIBLID [0211-8327 (2008) 44 (1); 91-140] RESUMEN: El estudio de los pectínidos (Bivalvia, Mollusca) en sedimentos pliocenos de la Cuenca de Vejer de la Frontera (Cádiz, SO España) permite determinar 13 especies, agrupadas en 8 géneros, ampliando la información previa en la zona de esta familia de bivalvos en 5 especies. La presencia de M. pesfelis, F. flexuosus, P. excisum, P. jacobaeus y P. maximus nos permite confirmar y corroborar la edad de Plioceno aportada por la microfauna. A su vez, la existencia de M. latissima, P. benedictus y P. excisum nos permite acotar la posición cronoestratigráfica hasta cerca de los 3,0 Ma. Las asociaciones dominantes en los sedimentos pliocenos apuntan a medios marinos someros, con fondos detríticos y energías variables, sometidos a la acción de tormentas, corroborado por la impronta tafonómica, como pueden ser sistemas de playa- duna y ambientes submareales donde se desarrollan barras y canales. Palabras clave: Pectinidae, Bivalvia, Plioceno, Cuenca de Vejer, Cádiz, SO España. ABSTRACT: This study has been carried out in pectinids (Bivalvia, Mollusca) of pliocene sediments from Vejer de la Frontera basin (Cádiz, SW Spain). The main results of this research has been the taxonomic determination of 8 genders and 13 species, rising previous pectinids information in this zone. -
John Mason Clarke
NATIONAL ACADEMY OF SCIENCES BIOGRAPHICAL MEMOIRS VOLUME XII'—SIXTH MEMOIR BIOGRAPHICAL MEMOIR OF JOHN MASON CLARKE BY CHARLES SCHUCHERT PRESENTED TO THE ACADEMY AT THE ANNUAL MEETING, 1926 JOHN MASON CLARKE BY CHARLES SCIIUCHERT In the death of John Mason Clarke, America loses its most brilliant, eloquent, and productive paleontologist, and the world its greatest authority on Devonian life and time. Author of more than 10,000 printed pages, distributed among about 450 books and papers, of which 300 deal with Geology, his efforts had to do mostly with pure science, and he often lamented, in the coming generation of doers, the lack of an adequate apprecia- tion of wondrous nature as recorded on the tablets of the earth's crust. He was peculiarly the child of his environment; born on Devonian rocks replete with fossils, in a home of high ideals and learning, situated in a state that has long appreciated science, he rose into the grandeur of geologic knowledge that was his. Clarke is survived by his wife, formerly Mrs. Fannie V. Bosler, of Philadelphia; by Noah T. Clarke, a son by his first wife, who was Mrs. Emma Sill (nee Juel), of Albany; by two stepdaughters, Miss Marie Bosler and Mrs. Edith (Sill) Humphrey, and a stepson, Mr. Frank N. Sill. Out of a family of six brothers and sisters, four remain to mourn his going: Miss Clara Mason Clarke, who, with Mr. S. Merrill Clarke, for many years city editor of the New York Sun, is living in the old homestead at Canandaigua ; Rev. Lorenzo Mason Clarke, pastor of the First Presbyterian Church of Brooklyn; and Mr. -
Lead, Zinc, and Fluorspar Deposits
A, Economic Geology, 46 Professional Paper No. 36 B, Descriptive Geology, 58 ( C, Systematic Geology and Paleontology, 71 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DlKECTOK THE LEAD, ZINC, AND FLUORSPAR DEPOSITS OF WESTERN KENTUCKY BY E. o. and W. S. TANGKLER SMITH WASHINGTON GOVERNMENT PRINTING OFFICE 1905 CONTENTS. Page. LETTER OF TRANSMITTAL, BY C. W. HAYES...... ........................................... 5 PART I. GEOLOGY AND GENERAL RELATIONS, BY E. 0. ULRICH............................... 7 PART II. ORE DEPOSITS AND MINES, BY W. S. TANGIER SMITH ............................... 107 INDEZ.........................................J.......................................... 209 LETTER OF TRANSMITTAL DEPARTMENT OF THE INTERIOR, UNITED STATES GEOLOGICAL SURVEY, Washington, D. C., June 8, 1904- SIR: I have the honor to transmit herewith the manuscript of a report on " The lead, zinc, and fluorspar deposits of western Kentucky," by E. O. Ulrich and W. S. Tangier Smith, and to recommend its publication as a professional paper. Field work was carried on during the summer of 1902 under cooperative agreement with the State Survey of Kentucky, and a brief summary of the results was published in Bulletin No. 213, ''Contributions to Economic Geology for 1902." Prior to the investigation in 1902, however, Mr. Ulrich spent the greater part of two years (1889 and 1890) in the same territory, while attached to the Geological Survey of Kentucky. The field was again visited by Mr. Ulrich in 1903, and the results of all these studies are brought together in this paper. The district is one of peculiar interest,, having a complicated fault structure and unique lithologic and mineralogic associations. While the report contains much matter of purely scientific interest, it has been prepared with especial reference to the needs of the mining industry, and in such form that its conclusions should be of great practical benefit in developing the industry in this district. -
An Annotated Checklist of the Marine Macroinvertebrates of Alaska David T
NOAA Professional Paper NMFS 19 An annotated checklist of the marine macroinvertebrates of Alaska David T. Drumm • Katherine P. Maslenikov Robert Van Syoc • James W. Orr • Robert R. Lauth Duane E. Stevenson • Theodore W. Pietsch November 2016 U.S. Department of Commerce NOAA Professional Penny Pritzker Secretary of Commerce National Oceanic Papers NMFS and Atmospheric Administration Kathryn D. Sullivan Scientific Editor* Administrator Richard Langton National Marine National Marine Fisheries Service Fisheries Service Northeast Fisheries Science Center Maine Field Station Eileen Sobeck 17 Godfrey Drive, Suite 1 Assistant Administrator Orono, Maine 04473 for Fisheries Associate Editor Kathryn Dennis National Marine Fisheries Service Office of Science and Technology Economics and Social Analysis Division 1845 Wasp Blvd., Bldg. 178 Honolulu, Hawaii 96818 Managing Editor Shelley Arenas National Marine Fisheries Service Scientific Publications Office 7600 Sand Point Way NE Seattle, Washington 98115 Editorial Committee Ann C. Matarese National Marine Fisheries Service James W. Orr National Marine Fisheries Service The NOAA Professional Paper NMFS (ISSN 1931-4590) series is pub- lished by the Scientific Publications Of- *Bruce Mundy (PIFSC) was Scientific Editor during the fice, National Marine Fisheries Service, scientific editing and preparation of this report. NOAA, 7600 Sand Point Way NE, Seattle, WA 98115. The Secretary of Commerce has The NOAA Professional Paper NMFS series carries peer-reviewed, lengthy original determined that the publication of research reports, taxonomic keys, species synopses, flora and fauna studies, and data- this series is necessary in the transac- intensive reports on investigations in fishery science, engineering, and economics. tion of the public business required by law of this Department. -
An Inventory of Trilobites from National Park Service Areas
Sullivan, R.M. and Lucas, S.G., eds., 2016, Fossil Record 5. New Mexico Museum of Natural History and Science Bulletin 74. 179 AN INVENTORY OF TRILOBITES FROM NATIONAL PARK SERVICE AREAS MEGAN R. NORR¹, VINCENT L. SANTUCCI1 and JUSTIN S. TWEET2 1National Park Service. 1201 Eye Street NW, Washington, D.C. 20005; -email: [email protected]; 2Tweet Paleo-Consulting. 9149 79th St. S. Cottage Grove. MN 55016; Abstract—Trilobites represent an extinct group of Paleozoic marine invertebrate fossils that have great scientific interest and public appeal. Trilobites exhibit wide taxonomic diversity and are contained within nine orders of the Class Trilobita. A wealth of scientific literature exists regarding trilobites, their morphology, biostratigraphy, indicators of paleoenvironments, behavior, and other research themes. An inventory of National Park Service areas reveals that fossilized remains of trilobites are documented from within at least 33 NPS units, including Death Valley National Park, Grand Canyon National Park, Yellowstone National Park, and Yukon-Charley Rivers National Preserve. More than 120 trilobite hototype specimens are known from National Park Service areas. INTRODUCTION Of the 262 National Park Service areas identified with paleontological resources, 33 of those units have documented trilobite fossils (Fig. 1). More than 120 holotype specimens of trilobites have been found within National Park Service (NPS) units. Once thriving during the Paleozoic Era (between ~520 and 250 million years ago) and becoming extinct at the end of the Permian Period, trilobites were prone to fossilization due to their hard exoskeletons and the sedimentary marine environments they inhabited. While parks such as Death Valley National Park and Yukon-Charley Rivers National Preserve have reported a great abundance of fossilized trilobites, many other national parks also contain a diverse trilobite fauna. -
Literature Cited
167 Literature cited Andersen, S., Burnetll, G. & Bergh, O. 2000. Flow-through systems for culturing great scallop larvae. Aquaculture International, 8: 249–257. Ansell, A.D. 1961. Reproduction, growth and mortality of Venus striatula (da Costa) in Kames Bay, Millport. J. Mar. Biol. Assoc. U.K., 41: 191–215. Barber, B. & Blake, N.J. 1983. Growth and reproduction of the bay scallop, Argopecten irradians (Lamarck) at its southern distributional limit. J. Exp. Mar. Biol. Ecol., 66: 247–256. Bayne, B.L. 1965. Growth and the delay of metamorphosis of the larvae of Mytilus edulis (L.). Ophelia, 2(1): 1–47. Bayne, B.L. 1983. Physiological ecology of marine molluscan larvae. In The Mollusca. Verdonk, N.H., Van den Biggelaar, J.A.M. & Tompa, A.S., eds. Vol. 3, Development. New York, Academic Press. pp. 299–343. Beaumont, A. R. & Budd, M.D. 1983. Effects of self-fertilization and other factors on the early development of the scallop Pecten maximus. Mar. Biol., 76: 285–289. Blake, N.J. & Moyer, M.A. 1991. The calico scallop, Argopecten gibbus, fishery of Cape Canaveral, Florida. In Scallops: Biology, Ecology, and Aquaculture. S. Shumway, ed. Elsevier, New York. pp. 899–909. Bourne, N. & Hodgson, C.A. 1991. Development of a viable nursery system for scallop culture. In International Compendium of Scallop Biology and Culture. S. Shumway & P. Sandifer, eds. The World Aquaculture Society, Louisiana State University, Baton Rouge, LA 70803. pp 273–280. Bourne, N., Hodgson, C.A. & Whyte, J.N.C. 1989. A manual for scallop culture in British Columbia. Canadian Technical Report of Fisheries and Aquatic Sciences. -
Upper Cretaceous (Maestrichtian) Mollusca from the Haustator Bilira Assemblage Zone in the East Gulf Coastal Plain
UNITED STATES DEPARTMENT OF INTERIOR GEOLOGICAL SURVEY Upper Cretaceous (Maestrichtian) Mollusca from the Haustator bilira Assemblage Zone in the East Gulf Coastal Plain Norman F. So hi 1 and Carl F. Koch2 Open File Feport 83-451 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial Standards and stratigraphic nomenclature. Pages are numbered one to four and seven to 239. 1. Washington D.C. 2. Old Dominion University Norfolk, Va, 1983 CONTENTS Page Introduction 1 Explanation 1 Explanation of Annotation 4 References 9 Molluscan Faunal Lists 11 ILLUSTRATIONS Figure 1 Map showing location of collections 2 Relationships of stratigraphic units within the Haustator bilira Assemblage Zone, East Gulf Coastal Plain TABLE Table 1 U.S. Geological Survey numbers of collections for each location Upper Cretaceous (Maestrichtian) Mollusca from the Haustator bilira Assemblage Zone in the East Gulf Coastal Plain INTRODUCTION The following report contains lists of the molluscan fauna from 189 collections made at 161 localities or different levels at a locality in the rocks of the Haustator bilira Assemblage Zone as exposed in western Georgia, Alabama, Mississippi, and Tennessee (Figure 1). This compilation forms the data base for a series of studies published, in press or in preparation (Buzas, £t_ al. , 1982; Koch and Sohl, in press). The Haustator bilira Assemblage Zone was proposed by Sohl (1977) and traced through Late Cretaceous rocks of the Atlantic and Gulf Coastal Plains from New Jersey to Texas (Owens, et_jil_., 1977; Sohl and Smith, 1980). The base of the zone occurs above the base of the foraminiferid Globotruncana gansseri subzone of Pessagno (1967) and includes all subsequent younger Cretaceous deposits on the Coastal Plains (Figure 2).